CN108205164A - A kind of atmospheric visibility parametrization Forecasting Methodology based on WRF-Chem - Google Patents

A kind of atmospheric visibility parametrization Forecasting Methodology based on WRF-Chem Download PDF

Info

Publication number
CN108205164A
CN108205164A CN201711259479.0A CN201711259479A CN108205164A CN 108205164 A CN108205164 A CN 108205164A CN 201711259479 A CN201711259479 A CN 201711259479A CN 108205164 A CN108205164 A CN 108205164A
Authority
CN
China
Prior art keywords
wrf
atmospheric
chem
scheme
visibility
Prior art date
Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
Pending
Application number
CN201711259479.0A
Other languages
Chinese (zh)
Inventor
高嵩
毕晓甜
赵天良
梁伟
朱孟周
张龙
Current Assignee (The listed assignees may be inaccurate. Google has not performed a legal analysis and makes no representation or warranty as to the accuracy of the list.)
State Grid Corp of China SGCC
Nanjing University of Information Science and Technology
Electric Power Research Institute of State Grid Jiangsu Electric Power Co Ltd
Original Assignee
State Grid Corp of China SGCC
Nanjing University of Information Science and Technology
Electric Power Research Institute of State Grid Jiangsu Electric Power Co Ltd
Priority date (The priority date is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the date listed.)
Filing date
Publication date
Application filed by State Grid Corp of China SGCC, Nanjing University of Information Science and Technology, Electric Power Research Institute of State Grid Jiangsu Electric Power Co Ltd filed Critical State Grid Corp of China SGCC
Priority to CN201711259479.0A priority Critical patent/CN108205164A/en
Publication of CN108205164A publication Critical patent/CN108205164A/en
Pending legal-status Critical Current

Links

Classifications

    • GPHYSICS
    • G01MEASURING; TESTING
    • G01WMETEOROLOGY
    • G01W1/00Meteorology
    • G01W1/10Devices for predicting weather conditions

Landscapes

  • Environmental & Geological Engineering (AREA)
  • Engineering & Computer Science (AREA)
  • Life Sciences & Earth Sciences (AREA)
  • Atmospheric Sciences (AREA)
  • Biodiversity & Conservation Biology (AREA)
  • Ecology (AREA)
  • Environmental Sciences (AREA)
  • Organic Low-Molecular-Weight Compounds And Preparation Thereof (AREA)

Abstract

The invention discloses a kind of atmospheric visibilities based on WRF Chem to parameterize Forecasting Methodology, obtains meteorological data and topographic(al) data in simulated time, sets assessment area and meteorological data and topographic(al) data are pre-processed;It selects to combine to simulating the different parameters scheme with larger impact, suitable Parameterization Scheme is selected according to simulation area;WRF Chem are run, using WRF Chem pattern simulation particle concentrations, according to Mie theoretical calculations particulate matter to the extinction coefficient of 550 nm, and consider the delustring of atmospheric molecule, atmospheric visibility is calculated with improved atmospheric visibility Parameterization Scheme.Due to combining at present research pair both at home and abroadKValue is corrected, and atmospheric extinction coefficient considers particulate matter extinction coefficient and gas molecular extinction coefficient simultaneously, and this method more can be derived that more accurate atmospheric visibility.

Description

A kind of atmospheric visibility parametrization Forecasting Methodology based on WRF-Chem
Technical field
The invention belongs to atmospheric environment pattern technology fields, and in particular to a kind of atmospheric visibility ginseng based on WRF-Chem Numberization Forecasting Methodology.
Background technology
Atmospheric visibility characterizes atmospheric transparency, can reflect the clean level of Air Close To The Earth Surface, with social life and Traffic safety is closely related.Since existing atmosphere pollution observation time sequence is shorter, the observation and analysis of atmospheric visibility It is still the main path of understanding atmospheric environment longer term climatic variation characteristic at present.The forecasting procedure of atmospheric visibility mainly has system Meter forecast and numerical forecast.Statistical fluctuation changes generally by analysis mist, atmospheric visibility of the haze when weather phenomena occur Rule establishes the statistical relationship of the meteorological elements such as temperature, humidity, wind speed, pressure and atmospheric visibility, establishes atmospheric visibility Prognostic equation numerical forecast mainly utilizes the elements such as pollutant, humidity, the Liquid water content in numerical model simulated atmosphere, according to According to atmospheric optics theory, its contribution to atmospheric extinction, diagnosis forecast atmospheric visibility are calculated.
At present, domestic and international main atmospheric visibility computational methods are the relation formulas of atmospheric visibility and extinction coefficient, I.e. object visual range theory atmospheric extinction coefficient is mainly proposed by IMPROVE projects (U.S.'s large size visibility surveillance program) IMPROVE empirical equations calculate.CHEN etc. by Tianjin Wuqing area atmospheric visibility to aerosol fraction and suction A kind of sensitivity analysis of wet growth factor, it is proposed that the Parameterization Scheme that low visibility delustring calculates under haze weather.Kunkel Deng passing through mist observation experiment in 1984, it is proposed that the relational expression of atmospheric visibility and Liquid water content.Gultepe etc. gives Atmospheric visibility formula based on fog content and droplet concentration.ZHOU etc. gives liquid water on the basis of radiation fog is studied The diagnostic method of content (LWC), and then propose the atmospheric visibility DATA PROCESSING IN ENSEMBLE PREDICTION SYSTEM method of mist.
For being now widely used in the WRF-Chem isotypes of air quality model forecast, existing calculating atmospheric visibility Parameterization Scheme availability it is not high, cause pattern poor to the computational accuracy of atmospheric visibility.
Invention content
Purpose:In order to overcome the deficiencies in the prior art, the present invention provides a kind of air energy based on WRF-Chem Degree of opinion parameterizes Forecasting Methodology, realizes the coupling of atmospheric visibility Parameterization Scheme and WRF-Chem patterns, this method can be more Add the prediction for accurately carrying out atmospheric visibility.
Technical solution:In order to solve the above technical problems, the technical solution adopted by the present invention is:
A kind of atmospheric visibility parametrization Forecasting Methodology based on WRF-Chem, which is characterized in that include the following steps:
(1) meteorological data and topographic(al) data in simulated time are obtained, assessment area is set and to meteorological data and landform Data is pre-processed;
(2) selection is combined to simulating the different parameters scheme with larger impact, suitable according to simulation area selection Parameterization Scheme;
Specifically, the Parameterization Scheme includes Microphysical scheme, long-wave radiation Parameterization Scheme, Shortwave radiative parameter Scheme, land surface scheme, Different Boundary Layer Parameterization Schemes, Convective Parameterization Schemes, aerosol scheme gas-phase chemical reaction Mechanism.
(3) using WRF-Chem pattern simulation particle concentrations, according to delustring of the Mie theoretical calculations particulate matter to 550nm Coefficient, and consider the delustring of atmospheric molecule, calculate atmospheric visibility with improved atmospheric visibility Parameterization Scheme.
Atmospheric visibility VRCalculation formula be:
In formula:bpFor particulate matter extinction coefficient, unit Mm-1;bsgFor gas molecule scattering coefficient, unit Mm-1;bagFor gas Body molecular absorption coefficient, unit Mm-1
Particulate matter extinction coefficient is extinction coefficient of the particulate matter to 550nm wavelength, is obtained by Mie theoretical calculations, formula It is as follows:
In formula:I is grain size section, value 1,2,3,4, corresponding grain size is respectively 0.039~0.156,0.156~ 0.625th, 0.625~2.5,2.5~10 μm;QextFor extinction efficiency factor;DpFor the average diameter of particulate matter, m;N is particulate matter Particle density, a/m3;voldryFor the volume fraction of dry particl object, %;volwaterFor liquid water volume fraction, %.
bsgFor the Rayleigh scattering of gas molecule scattering coefficient, mainly atmospheric molecule, constant is usually regarded as, it is preferred that bsg Value is 13Mm-1
bagFor gas molecules sorb coefficient, mainly by NO2Pollution contribution, absorption coefficient are about NO2Mass concentration 0.33 times.
Advantageous effect:Atmospheric visibility parametrization Forecasting Methodology provided by the invention based on WRF-Chem, based on existing The total extinction coefficient of air and atmospheric visibility relationship, with reference to east China air quality and atmospheric visibility observational study, According to Mie theories and the Extinction Characteristic of atmospheric molecule, particulate matter and NO are calculated2Extinction coefficient, propose a kind of improved air Visibility Parameterization Scheme, and atmospheric extinction coefficient considers particulate matter extinction coefficient and gas molecular extinction coefficient simultaneously, Gas molecule extinction coefficient is the sum of gas molecule scattering coefficient and gas molecular absorption coefficient.It is said from overall numerical procedure, it should Pattern is to calculate the preferable selection of atmospheric visibility.
With Nanjing of China 25 days-December 10 November in 2013 and two haze contamination accidents on December 20-29th, 2013 Example shows the Average normalized deviation and average deviation of two hazes pollution example visibility of modified scheme simulation In respectively 17.19%, 3.18% and 517m, 173m, and and observation visibility related coefficient be respectively increased to 0.76, 0.87, the accuracy of visibility simulation better than other two kinds of existing Parameterization Schemes, and in different relative humidity (RH) and The standardization mean error that modified scheme is simulated in visibility range is respectively less than other two kinds of Parameterization Schemes, wherein In RH < 80% and visibility >=1km range internal standardization mean errors less than 50%.The improved air of the present invention can be shown in Degree Parameterization Scheme can effectively improve the forecast accuracy of the haze pollution ambient air visibility of air quality model.
Description of the drawings
Fig. 1 is the method for the present invention flow chart;
Fig. 2 is the comparison of three kinds of parametrization program simulation visibility and observation in the different haze pollution periods;
Fig. 3 is three kinds of parametrization program simulation results in different visibility scales and the average deviation of humidity range;
Fig. 4 is that three kinds of parametrization program simulation results are averagely missed in the standardization of different visibility scales and humidity range Difference.
Specific embodiment
With reference to embodiment, the invention will be further described.Following embodiment is only used for clearly illustrating this hair Bright technical solution, and be not intended to limit the protection scope of the present invention and limit the scope of the invention.
As shown in Figure 1, a kind of atmospheric visibility parametrization Forecasting Methodology based on WRF-Chem, includes the following steps:It obtains Meteorological data and topographic(al) data in the modulus pseudotime set assessment area and meteorological data and topographic(al) data are located in advance Reason.
It selects to combine to simulating the different parameters scheme with larger impact, suitable parameter is selected according to simulation area Change scheme.
It is as follows using the grid setting of WRF-Chem3.7 version analog studies:Vertical direction is divided into 28 layers, and top of model is 100hPa;Horizontal direction sets three layers of nested grid, resolution ratio ecto-entad is respectively 45,15,5km, covering China is absolutely successively Most area, East China and Central China some areas, Jiangsu Province and Anhui Zhejiang some areas;Regional center be located at Nanjing (32 ° of N, 118°E).Table 1 gives the physical and chemical process Parameterization Scheme in pattern simulation setting.Emission inventory is used by population INTEX-B data in 2006 after distribution, chemical initial fields use MOZART, simulate 25 days-December of November in 2013 10 respectively Day and two haze contamination accidents on December 20-29th, 2013.
WRF-Chem mode parameters scheme setting such as following table:
Scheme type Pattern options
Microphysical scheme Morrison schemes
Long-wave radiation Parameterization Scheme RRTM schemes
Shortwave radiative parameter scheme RRTM schemes
Land surface scheme Noah schemes
Different Boundary Layer Parameterization Schemes YSU schemes
Convective Parameterization Schemes Grell 3D schemes
Aerosol scheme MOSAIC schemes
Gas-phase chemical reaction mechanism CBMZ mechanism
WRF-Chem is run, using WRF-Chem pattern simulation particle concentrations, according to Mie theoretical calculation particulate matters pair The extinction coefficient of 550nm, and consider the delustring of atmospheric molecule, it is counted with improved atmospheric visibility Parameterization Scheme (scheme C) Calculate atmospheric visibility.And compared with the visibility Parameterization Scheme (option b) of existing IMPROVE schemes (option A) and CHEN, As a result such as following table:
The atmospheric visibility that scheme C (improved atmospheric visibility Parameterization Scheme) is simulated it can be seen from analog result With observe it is closest, average deviation and standardization average deviation be minimum, respectively 517m, 17.19%, for it is entire when Between section simulation effect it is best.Atmospheric visibility moulds of the scheme C (improved atmospheric visibility Parameterization Scheme) within the entire period Intend deviation to be substantially reduced, simulation is the most accurate, and related coefficient is up to 0.87, and average deviation is only 173m, standardizes average deviation It is respectively 3.18%, 27.16% with standardization mean error.
Fig. 2 is the comparison of three kinds of parametrization program simulation visibility and observation in the different haze pollution periods;As seen from the figure, Scheme C (improved atmospheric visibility Parameterization Scheme) and measured value are integrally closest, are better than and option A (IMPROVE side Case) and option b (the visibility Parameterization Scheme of CHEN) result of calculation, scheme C (improved atmospheric visibility parametrization sides Case) it can effectively improve the accuracy in computation of atmospheric visibility.
Fig. 3 is three kinds and parameterizes program simulation results in different visibility scales and the average deviation of humidity range, and Fig. 4 is Three kinds of parametrization program simulation results are in different visibility scales and the standardization mean error of humidity range.
Scheme C is under the conditions of each visibility range and different RH to the possesses good fitting of atmospheric visibility, average deviation and mark Standardization mean error is minimum, and optical principle Mie theoretical calculation particulate matter extinction coefficients are based on better than other two schemes schemes C, Consider the Extinction Characteristic of atmospheric molecule, diagnosis obtains visibility, and result is more accurate, reasonable on the whole.
The above is only the preferred embodiment of the present invention, it should be pointed out that:For the ordinary skill people of the art For member, various improvements and modifications may be made without departing from the principle of the present invention, these improvements and modifications also should It is considered as protection scope of the present invention.

Claims (6)

1. a kind of atmospheric visibility parametrization Forecasting Methodology based on WRF-Chem, which is characterized in that include the following steps:
(1) meteorological data and topographic(al) data in simulated time are obtained, assessment area is set and to meteorological data and topographic(al) data It is pre-processed;
(2) selection is combined to simulating the different parameters scheme with larger impact, and suitable parameter is selected according to simulation area Change scheme;
(3) using WRF-Chem pattern simulation particle concentrations, according to Mie theoretical calculations particulate matter to the extinction coefficient of 550nm, And consider the delustring of atmospheric molecule, calculate atmospheric visibility with improved atmospheric visibility Parameterization Scheme.
2. the atmospheric visibility parametrization Forecasting Methodology according to claim 1 based on WRF-Chem, it is characterised in that:Institute It states Parameterization Scheme and includes Microphysical scheme, long-wave radiation Parameterization Scheme, Shortwave radiative parameter scheme, land surface emissivity side Case, Different Boundary Layer Parameterization Schemes, Convective Parameterization Schemes, aerosol scheme gas-phase chemical reaction mechanism.
3. the atmospheric visibility parametrization Forecasting Methodology according to claim 1 based on WRF-Chem, it is characterised in that:Greatly Gas visibility VRCalculation formula be:
In formula:bpFor particulate matter extinction coefficient, unit Mm-1;bsgFor gas molecule scattering coefficient, unit Mm-1;bagFor gas point Sub- absorption coefficient, unit Mm-1
4. the atmospheric visibility parametrization Forecasting Methodology according to claim 3 based on WRF-Chem, it is characterised in that: Grain object extinction coefficient is extinction coefficient of the particulate matter to 550nm wavelength, is obtained by Mie theoretical calculations, formula is as follows:
In formula:I is grain size section, value 1,2,3,4, corresponding grain size is respectively 0.039~0.156,0.156~0.625, 0.625~2.5,2.5~10 μm;QextFor extinction efficiency factor;DpFor the average diameter of particulate matter, m;N is that the number of particulate matter is dense Degree, a/m3;voldryFor the volume fraction of dry particl object, %;volwaterFor liquid water volume fraction, %.
5. the atmospheric visibility parametrization Forecasting Methodology according to claim 3 based on WRF-Chem, it is characterised in that:bsg Value is 13Mm-1
6. the atmospheric visibility parametrization Forecasting Methodology according to claim 3 based on WRF-Chem, it is characterised in that:bag For gas molecules sorb coefficient, mainly by NO2Pollution contribution, absorption coefficient NO20.33 times of mass concentration.
CN201711259479.0A 2017-12-04 2017-12-04 A kind of atmospheric visibility parametrization Forecasting Methodology based on WRF-Chem Pending CN108205164A (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
CN201711259479.0A CN108205164A (en) 2017-12-04 2017-12-04 A kind of atmospheric visibility parametrization Forecasting Methodology based on WRF-Chem

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
CN201711259479.0A CN108205164A (en) 2017-12-04 2017-12-04 A kind of atmospheric visibility parametrization Forecasting Methodology based on WRF-Chem

Publications (1)

Publication Number Publication Date
CN108205164A true CN108205164A (en) 2018-06-26

Family

ID=62604664

Family Applications (1)

Application Number Title Priority Date Filing Date
CN201711259479.0A Pending CN108205164A (en) 2017-12-04 2017-12-04 A kind of atmospheric visibility parametrization Forecasting Methodology based on WRF-Chem

Country Status (1)

Country Link
CN (1) CN108205164A (en)

Cited By (8)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN109444986A (en) * 2018-09-30 2019-03-08 国网天津市电力公司电力科学研究院 A kind of photovoltaic power station foggy weather visibility prediction technique
CN109543906A (en) * 2018-11-23 2019-03-29 长三角环境气象预报预警中心(上海市环境气象中心) A kind of method and apparatus of atmospheric visibility prediction
CN109597969A (en) * 2019-01-25 2019-04-09 南京大学 A kind of surface ozone Concentration Estimation Method
CN109932988A (en) * 2019-03-27 2019-06-25 四川瞭望工业自动化控制技术有限公司 A kind of city raised dust contamination forecasting system and method
CN111382506A (en) * 2020-03-02 2020-07-07 苏州工业园区洛加大先进技术研究院 Method for evaluating influence of aerosol and radiation interaction on atomization effect
CN111398109A (en) * 2020-03-10 2020-07-10 上海眼控科技股份有限公司 Atmospheric visibility measuring method, sensor module, system and storage medium
CN115204507A (en) * 2022-07-26 2022-10-18 北京中科三清环境技术有限公司 Atmospheric visibility prediction method, device, equipment and storage medium
CN117554992A (en) * 2024-01-10 2024-02-13 青岛镭测创芯科技有限公司 Extinction coefficient acquisition method and system based on laser radar

Non-Patent Citations (2)

* Cited by examiner, † Cited by third party
Title
胡俊,赵天良,张泽锋,邱玉珺,谭成好,吴峡生等: "霾污染环境大气能见度参数化方案的改进", 《环境科学研究》 *
荣昕: "基于WRF-CHEM模式的连续雾霾过程数值模拟及其能见度参数化", 《基础科学辑》 *

Cited By (12)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN109444986A (en) * 2018-09-30 2019-03-08 国网天津市电力公司电力科学研究院 A kind of photovoltaic power station foggy weather visibility prediction technique
CN109444986B (en) * 2018-09-30 2021-01-19 国网天津市电力公司电力科学研究院 Visibility prediction method for foggy weather of distributed photovoltaic power station
CN109543906A (en) * 2018-11-23 2019-03-29 长三角环境气象预报预警中心(上海市环境气象中心) A kind of method and apparatus of atmospheric visibility prediction
CN109543906B (en) * 2018-11-23 2024-04-16 长三角环境气象预报预警中心(上海市环境气象中心) Atmospheric visibility prediction method and equipment
CN109597969A (en) * 2019-01-25 2019-04-09 南京大学 A kind of surface ozone Concentration Estimation Method
CN109932988A (en) * 2019-03-27 2019-06-25 四川瞭望工业自动化控制技术有限公司 A kind of city raised dust contamination forecasting system and method
CN109932988B (en) * 2019-03-27 2020-11-24 四川瞭望工业自动化控制技术有限公司 Urban raise dust pollution diffusion prediction system and method
CN111382506A (en) * 2020-03-02 2020-07-07 苏州工业园区洛加大先进技术研究院 Method for evaluating influence of aerosol and radiation interaction on atomization effect
CN111398109A (en) * 2020-03-10 2020-07-10 上海眼控科技股份有限公司 Atmospheric visibility measuring method, sensor module, system and storage medium
CN115204507A (en) * 2022-07-26 2022-10-18 北京中科三清环境技术有限公司 Atmospheric visibility prediction method, device, equipment and storage medium
CN117554992A (en) * 2024-01-10 2024-02-13 青岛镭测创芯科技有限公司 Extinction coefficient acquisition method and system based on laser radar
CN117554992B (en) * 2024-01-10 2024-04-09 青岛镭测创芯科技有限公司 Extinction coefficient acquisition method and system based on laser radar

Similar Documents

Publication Publication Date Title
CN108205164A (en) A kind of atmospheric visibility parametrization Forecasting Methodology based on WRF-Chem
Tang et al. Impact of emission controls on air quality in Beijing during APEC 2014: lidar ceilometer observations
Soegaard et al. Towards a spatial CO2 budget of a metropolitan region based on textural image classification and flux measurements
Yan et al. The measurement of aerosol optical properties at a rural site in Northern China
Xiang-Ao et al. Aerosol properties and their spatial and temporal variations over North China in spring 2001
Hoffmann et al. Effects of grazing and topography on dust flux and deposition in the Xilingele grassland, Inner Mongolia
Quinn et al. Comparison of measured and calculated aerosol properties relevant to the direct radiative forcing of tropospheric sulfate aerosol on climate
CN104897853A (en) Thermal power plant pollutant discharging monitoring display method based on tower type diffusion model
CN110929228B (en) Inversion algorithm for moisture absorption growth factor of uniformly mixed aerosol
Goossens et al. Techniques to measure the dry aeolian deposition of dust in arid and semi‐arid landscapes: a comparative study in West Niger
CN107561554A (en) Inversion method with multi-wavelength laser radar data is counted based on solar luminosity
CN112180472A (en) Atmospheric visibility integrated forecasting method based on deep learning
CN103234882B (en) A kind of Atmospheric particulates mass concentration inversion method based on the particulate matter flight time
CN103336995A (en) Method for constructing real-time light metering network of million kilowatt level photovoltaic power generation base
Zhou et al. Improving aerosol interaction with clouds and precipitation in a regional chemical weather modeling system
Patterson et al. Monte Carlo simulation of daily regional sulfur distribution: comparison with SURE sulfate data and visual range observations during August 1977
CN108663727A (en) The method for estimating height of evaporation duct within the scope of world marine site using evaporation rate
Zou et al. Impact of eddy characteristics on turbulent heat and momentum fluxes in the urban roughness sublayer
Cleugh Field measurements of windbreak effects on airflow, turbulent exchanges and microclimates
CN110907319B (en) Attribution analysis method for near-surface fine particulate matters
Virkkula et al. The influence of Kola Peninsula, continental European and marine sources on the number concentrations and scattering coefficients of the atmospheric aerosol in Finnish Lapland
CN110907318B (en) Near-ground atmospheric total suspended particulate matter mass concentration remote sensing physical estimation method
CN109948175B (en) Satellite remote sensing albedo missing value inversion method based on meteorological data
CN109918770B (en) Artificial precipitation removal fine particle prediction model
KR101194677B1 (en) Estimation method of source of high concentration fine dust in urban area

Legal Events

Date Code Title Description
PB01 Publication
PB01 Publication
SE01 Entry into force of request for substantive examination
SE01 Entry into force of request for substantive examination
RJ01 Rejection of invention patent application after publication
RJ01 Rejection of invention patent application after publication

Application publication date: 20180626